Aerodynamic theory and empirical observations of animals flying at similar Reynolds numbers (Re) predict
that airflow over hummingbird wings will be dominated by a stable, attached leading edge vortex
(LEV). In insects exhibiting similar kinematics, when the translational movement of the wing ceases
(as at the end of the downstroke), the LEV is shed and lift production decreases until the energy of
the LEV is re-captured in the subsequent half-cycle translation. We here show that while the hummingbird
wing is strongly influenced by similar sharp-leading-edge aerodynamics, leading edge vorticity is
inconsistent, varying from 0.7 to 26 per cent (mean 16%) of total lift production, is always generated
within 3 mm of the dorsal surface of the wing, showing no retrograde (trai领 to leading edge) flow,
and does not increase from proximal to distal wing as would be expected with a conical vortex (class
III LEV) described for hawkmoths. Further, the bound circulation is not shed as a vortex at the end
of translation, but instead remains attached and persists after translation has ceased, augmented by the
rotation (pronation, supination) of the wing that occurs between the wing-translation half-cycles. The
result is a near-continuous lift production through wing turn-around, previously unknown in vertebrates,
able to contribute to weight support as well as stability and control during hovering. Selection for a planform
suited to creating this unique flow and nearly-uninterrupted lift production throughout the wingbeat
cycle may help explain the relatively narrow hummingbird wing. 德国LaVision PIV/PLIF粒子成像测速场仪
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